Figure 4
Map of the crust-mantle interface of Mercury predicted from a lithospheric flexure model, expressed as depth (km) with respect to the reference surface, in a Mollweide projection. We modeled the deflection of the crust-mantle interface using the estimated elastic lithosphere thickness of 30 km, the crustal thickness (Tc) of 35 km and the densities of 2800 kg/m3 and 3200 kg/m3, for crust and mantle respectively.
